Microbial oceanography of the dark ocean's pelagic realm

By J. Arístegui, J. Gasol, Carlos M. Duarte, Gerhard J. Herndld. 2009

460 citations recorded by the source corpus.

Subfields: Ecology, Environmental Chemistry, Oceanography

View Paper: https://www.semanticscholar.org/paper/c6aa9553a73c3d7507b5e4af0f32cbefc0618ce3

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In Environmental Chemistry

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Citations in the corpus

Viruses in aquatic ecosystems: important advancements of the last 20 years and prospects for the future in the field of microbial oceanography and limnology (2010, background): “High viral abundance is often found when prokaryotic host numbers are high as well [48,222].”
Major contribution of autotrophy to microbial carbon cycling in the deep North Atlantic’s interior (2010, background): “While geochemical measurements provide major insights into the general ocean carbon cycle, our mechanistic understanding of the dark ocean’s carbon cycle and the role of the microbial communities in the transformation of carbon remains rudimentary (Arı́stegui et al., 2009).”
Microbial Respiration, the Engine of Ocean Deoxygenation (2019, methodology): “, 2003), which were calculated using a conversion factor derived from a senescent bacterial culture, suggesting that microbial communities in the mesopelagic ocean are much more active that previously assumed (Arístegui et al., 2009).”
Beyond the Calvin cycle: autotrophic carbon fixation in the ocean. (2011, background): “The meso- and bathypelagic realms of the ocean represent the largest continuous habitats on Earth, yet we know very little about the kind of microbes living in these zones and the global impact of their activities (Aristegui et al. 2009).”
Dark inorganic carbon fixation sustains the functioning of benthic deep‐sea ecosystems (2013, background): “…imbalance between the OC supply and its consumption has been explained on the basis of potential underestimation of the allochthonous inputs of OC [Arístegui et al., 2009; Burd et al., 2010] and/or that of additional sources of OC that are produced in situ through chemoautotrophic processes…”
Structure and function of the global ocean microbiome (2015, unknown): “remineralization site of exported production (50).”
The biomass distribution on Earth (2018, background): “(29), and multiplied them by the surface area of the oceans (3.”
Microbial Surface Colonization and Biofilm Development in Marine Environments (2015, background): “The particle origin, degree of decomposition, nutritional status, and environmental temperature may determine the composition, succession, and activity of the sinking-particle-colonizing microbial community, which may select in favor of a surface-associated composition distinct from that of the free”
The Biological carbon pump in the North Atlantic (2014, background): “Aggregates are hot spots for bacterial activity (Alldredge et al., 1986; Aristegui et al., 2009).”
Mechanisms of Microbial Carbon Sequestration in the Ocean - Future Research Directions (2014, background): “This is supported by evidence suggesting that carbon-limited deep-ocean prokaryotes show a preferential particle-related life strategy (DeLong et al., 2006; Arístegui et al., 2009; Baltar et al., 2009, 2010b).”
Emerging concepts on microbial processes in the bathypelagic ocean-ecology, biogeochemistry, and genomics (2010, background): “The depth dependent pattern in full depth distributions of HNF can be described by a power function, with exponents being greater than those for prokaryotes (Tanaka and Rassoulzadegan, 2002; Arı́stegui et al., 2009).”